The continuous volcanic and seismic activity at Mount Etna makes this volcano an important laboratory for
seismological and geophysical studies. We used repeated three-dimensional tomography (4D tomography) to
detect variations in elastic parameters during different volcanic cycles in the period November 2000–May 2008,
that includes several flank eruptions.
The use of a large number of permanent seismic stations and the abundance of local earthquakes, occurring both
before and during the eruptions, guarantee consistent and high-resolution velocity models. First, we performed a
tomographic inversion of the whole data set to define the 3D P-wave velocity (VP) and the structure of the P- to
S-wave velocity ratio (VP/VS). A total of ca. 3,000 well constrained earthquakes (root mean square time residuals
0.4 s; horizontal and vertical hypocentral location errors 1.5 km; azimuthal gap of the stations 180 ), ca.
40,000 P-wave arrivals, and ca. 9,000 S-wave arrivals were inverted to model a grid, 2 km by 2 km by 1 km spaced,
with the use of SIMULPS-14 software. Then, on the basis of geophysical and geochemical observations indicating
some cyclic recharging and discharging (eruptions) phases, we inverted different sub-periods to investigate time
variations in the elastic parameters.
The observed time changes of velocity-oriented anomalies suggest that four-dimensional tomography could
provide a basis for more efficient volcano monitoring and short- and midterm eruption forecasting.